JURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENT
The intimate stratigraphical association between Lower Toarcian manganese carbonates and carbon-rich shales in Austria, Czechoslovakia, Germany, Hungary, Italy, and Switzerland is suggestive of a genetic connection between the two, given the similar anoxic to euxinic depositional environments in whi...
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Format: | Journal article |
Language: | English |
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1991
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author | Jenkyns, H Geczy, B Marshall, J |
author_facet | Jenkyns, H Geczy, B Marshall, J |
author_sort | Jenkyns, H |
collection | OXFORD |
description | The intimate stratigraphical association between Lower Toarcian manganese carbonates and carbon-rich shales in Austria, Czechoslovakia, Germany, Hungary, Italy, and Switzerland is suggestive of a genetic connection between the two, given the similar anoxic to euxinic depositional environments in which both these distinctive sediments form today. Ammonite biostratigraphy and carbon-isotope stratigraphy suggest that these metalliferous deposits are everywhere of identical age, namely tenuicostatum to early falciferum Zones. Recognition of an early Toarcian anoxic event in the Alpine-Mediterranean domain, characterized by the development of a well-developed oxygen-minimum zone across the rifted proto-continental margins of the Tethys, indicates that these metalliferous deposits can be related to mid-water transport of manganese, possibly of continental derivation. -from Authors |
first_indexed | 2024-03-07T05:07:29Z |
format | Journal article |
id | oxford-uuid:da6b2c7a-1ff5-4e88-ab05-8af625b15457 |
institution | University of Oxford |
language | English |
last_indexed | 2024-03-07T05:07:29Z |
publishDate | 1991 |
record_format | dspace |
spelling | oxford-uuid:da6b2c7a-1ff5-4e88-ab05-8af625b154572022-03-27T09:03:10ZJURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENTJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:da6b2c7a-1ff5-4e88-ab05-8af625b15457EnglishSymplectic Elements at Oxford1991Jenkyns, HGeczy, BMarshall, JThe intimate stratigraphical association between Lower Toarcian manganese carbonates and carbon-rich shales in Austria, Czechoslovakia, Germany, Hungary, Italy, and Switzerland is suggestive of a genetic connection between the two, given the similar anoxic to euxinic depositional environments in which both these distinctive sediments form today. Ammonite biostratigraphy and carbon-isotope stratigraphy suggest that these metalliferous deposits are everywhere of identical age, namely tenuicostatum to early falciferum Zones. Recognition of an early Toarcian anoxic event in the Alpine-Mediterranean domain, characterized by the development of a well-developed oxygen-minimum zone across the rifted proto-continental margins of the Tethys, indicates that these metalliferous deposits can be related to mid-water transport of manganese, possibly of continental derivation. -from Authors |
spellingShingle | Jenkyns, H Geczy, B Marshall, J JURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENT |
title | JURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENT |
title_full | JURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENT |
title_fullStr | JURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENT |
title_full_unstemmed | JURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENT |
title_short | JURASSIC MANGANESE CARBONATES OF CENTRAL-EUROPE AND THE EARLY TOARCIAN ANOXIC EVENT |
title_sort | jurassic manganese carbonates of central europe and the early toarcian anoxic event |
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